Abstract
The distribution and genesis of n-alkanes in sediments from the 38-m sequence obtained during core boring in the Ivashkina lagoon were studied. Sediments were formed in the Holocene as a result of thermokarst and penetration of seawater. The sequence mostly includes permafrost rocks partially molten in the upper horizons and covered by Quaternary deposits, which are mostly the products of thermoabrasion.
| Original language | English |
|---|---|
| Pages (from-to) | 36-39 |
| Number of pages | 4 |
| Journal | Doklady Earth Sciences |
| Volume | 472 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 1 Jan 2017 |
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ASJC Scopus subject areas
- Earth and Planetary Sciences (miscellaneous)
- Earth and Planetary Sciences(all)
Cite this
Alkanes in Quaternary deposits of the Laptev Sea. / Romankevich, E. A.; Vetrov, A. A.; Belyaev, N. A.; Sergienko, V. I.; Semiletov, I. P.; Sukhoverkhov, S. V.; Bratskaya, S. Yu; Prokuda, N. A.; Ulyantsev, A. S.
In: Doklady Earth Sciences, Vol. 472, No. 1, 01.01.2017, p. 36-39.Research output: Contribution to journal › Article
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TY - JOUR
T1 - Alkanes in Quaternary deposits of the Laptev Sea
AU - Romankevich, E. A.
AU - Vetrov, A. A.
AU - Belyaev, N. A.
AU - Sergienko, V. I.
AU - Semiletov, I. P.
AU - Sukhoverkhov, S. V.
AU - Bratskaya, S. Yu
AU - Prokuda, N. A.
AU - Ulyantsev, A. S.
PY - 2017/1/1
Y1 - 2017/1/1
N2 - The distribution and genesis of n-alkanes in sediments from the 38-m sequence obtained during core boring in the Ivashkina lagoon were studied. Sediments were formed in the Holocene as a result of thermokarst and penetration of seawater. The sequence mostly includes permafrost rocks partially molten in the upper horizons and covered by Quaternary deposits, which are mostly the products of thermoabrasion.
AB - The distribution and genesis of n-alkanes in sediments from the 38-m sequence obtained during core boring in the Ivashkina lagoon were studied. Sediments were formed in the Holocene as a result of thermokarst and penetration of seawater. The sequence mostly includes permafrost rocks partially molten in the upper horizons and covered by Quaternary deposits, which are mostly the products of thermoabrasion.
UR - http://www.scopus.com/inward/record.url?scp=85017585853&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85017585853&partnerID=8YFLogxK
U2 - 10.1134/S1028334X17010093
DO - 10.1134/S1028334X17010093
M3 - Article
VL - 472
SP - 36
EP - 39
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 1
ER -